| Literature DB >> 31584198 |
Jeroen Reneerkens1, Tom S L Versluijs1, Theunis Piersma1,2, José A Alves3,4, Mark Boorman5, Colin Corse6, Olivier Gilg7,8, Gunnar Thor Hallgrimsson9, Johannes Lang8,10, Bob Loos11, Yaa Ntiamoa-Baidu12,13, Alfred A Nuoh12, Peter M Potts14, Job Ten Horn2, Tamar Lok2.
Abstract
Evolutionary theories of seasonal migration generally assume that the costs of longer migrations are balanced by benefits at the non-breeding destinations. We tested, and rejected, the null hypothesis of equal survival and timing of spring migration for High Arctic breeding sanderling Calidris alba using six and eight winter destinations between 55°N and 25°S, respectively. Annual apparent survival was considerably lower for adult birds wintering in tropical West Africa (Mauritania: 0.74 and Ghana: 0.75) than in three European sites (0.84, 0.84 and 0.87) and in subtropical Namibia (0.85). Moreover, compared with adults, second calendar-year sanderlings in the tropics, but not in Europe, often refrained from migrating north during the first possible breeding season. During northward migration, tropical-wintering sanderlings occurred at their final staging site in Iceland 5-15 days later than birds wintering further north or south. Namibia-wintering sanderlings tracked with solar geolocators only staged in West Africa during southward migration. The low annual survival, the later age of first northward migration and the later passage through Iceland during northward migration of tropical-wintering sanderlings, in addition to the skipping of this area during northward but not southward migration by Namibia-wintering sanderlings, all suggest they face issues during the late non-breeding season in West Africa. Migrating sanderlings defy long distances but may end up in winter areas with poor fitness prospects. We suggest that ecological conditions in tropical West Africa make the fuelling prior to northward departure problematic.Entities:
Keywords: demography; fitness; migration; nutrient storage strategies; site fidelity; solar geolocation; survival; timing
Mesh:
Year: 2019 PMID: 31584198 PMCID: PMC7078868 DOI: 10.1111/1365-2656.13118
Source DB: PubMed Journal: J Anim Ecol ISSN: 0021-8790 Impact factor: 5.091
Figure 1(a) Locations where sanderlings, individually colour‐ringed at Zackenberg, a breeding site in northeast Greenland (white dot), were observed in winter (between 1 October and 31 March; red dots). The size of the red dots is indicative of the number of individuals. The dark yellow and light blue areas indicate the breeding location and the winter range of Greenlandic sanderlings (based on van de Kam, Ens, Piersma, & Zwarts, 2004, modified after Reneerkens et al., 2009). The grey horizontal lines indicate the zones of 5 degrees latitude which separate winter areas as used in our analyses. Winter areas in bold were analysed for both timing of northward migration and adult survival. (b–h) Seven tracks of six individual sanderlings equipped with a solar geolocator in northeast Greenland. Numbers in the right top of each panel are ring numbers, below which the years of southward (autumn) migration and northward (spring) migration are given. Two tracks in 2013–2014 and 2015–2016 of the same individual with ring number 8,223,401 are shown in separate, adjacent panels. Southward movements are indicated with black lines in which staging sites (stationary periods as indicated by FLightR) are downward triangles. Northward migration tracks are in orange, with upward triangles indicating staging sites. The size of the triangles indicates the length of the staging period. The sex of each tracked bird is shown in the lower left corner of each panel. Small white dots indicate the location of solar geolocator deployment and retrieval (i.e., Zackenberg, except for 8,214,904 which was ringed and recaptured at Karupelv Valley). (i) Dates at which individuals arrived in the Arctic (i.e., permanent daylight was recorded) in relation to the date of departure from the winter area for the six tracked sanderlings. Colour of the dots refers to winter areas in West Africa (yellow) or Namibia (purple) and letters in the dots to the corresponding tracks in panels b–h
Number of full‐grown individuals (i.e., excluding non‐fledged birds in Greenland) ringed and/or molecularly sexed per study site within the range of Greenlandic sanderlings. Season during which animals were caught refers to the breeding period (B; June–10 August in Greenland), the migration period (M;1 April ‐ 30 September outside Greenland) and in winter (W; 1 October–31 March). ‘n’ refers to the number of birds captured, ‘n marked’ refers to the number of birds that were individually colour‐ringed, and ‘n sexed’ refers to the number of individuals that were molecularly sexed. The winter area of individuals that were caught during the breeding period or during migration may or may not be known; see the different analyses within the Materials and Methods for sample sizes per winter area. Notice that in some studied winter areas, there was no main study site where birds were caught. Hence, no study sites in France and north Iberia are mentioned in this table
|
Location (country) |
Coordinates (decimal degrees) | Season |
Period (years) |
|
(%) |
(%) |
|---|---|---|---|---|---|---|
|
Hochstetter Forland (Greenland) | 75.16666, −19.75000 | B | 2010–2013 | 108 | 107 (99%) | 86 (80%) |
|
Zackenberg (Greenland) | 74.46665, −20.56684 | B | 2007–2013 | 268 | 267 (100%) | 263 (98%) |
|
Karupelv Valley (Greenland) | 72.49994, −23.99954 | B | 2011–2013 | 52 | 52 (100%) | 27 (52%) |
|
Sandgerði (Iceland) | 64.04261, −22.71404 | M | 2007–2013 | 1,218 | 1,205 (99%) | 560 (46%) |
|
Sanday (Scotland) | 59.24081, −2.51783 | M,W | 1987–2013 | 378 | 163 (43%) | 167 (44%) |
|
Wadden Sea (Netherlands) | 53.24967, 5.24271 | M, W | 2007–2013 | 750 | 505 (67%) | 285 (38%) |
|
Hayling Island (England) | 50.78336, −0.93620 | M,W | 2001–2013 | 103 | 103 (100%) | 0 (0%) |
|
Tagus estuary (Portugal) | 38.74658, −8.97778 | M,W | 2008–2013 | 382 | 381 (100%) | 13 (3%) |
|
Iwik, Banc d’Arguin (Mauritania) | 19.87754, −16.30356 | W | 2002–2013 | 1,483 | 1,302 (88%) | 922 (62%) |
|
Esiama (Ghana) | 4.92577, −2.33373 | M,W | 2007–2013 | 1,136 | 1,135 (100%) | 194 (21%) |
|
Swakopmund (Namibia) | −22.71218, 14.52589 | W | 1971–1979 | 34 | 0 (0%) | 0 (0%) |
Models for seasonal survival of adult sanderlings at six winter areas along the East Atlantic Flyway in 2007–2013. Of 40 candidate models, only those with ΔQAICc <65 are shown. Model parameterization is explained in Table S2. Models are ranked by ascending ΔQAICc, w is the model weight, and K is the number of parameters
| Model | QAICc | ΔQAICc |
|
| QDeviance |
|---|---|---|---|---|---|
| Φ(winter area) p(winter area*year*season) | 5,800 | 0 | 0.53 | 84 | 1,480 |
| Φ(winter area + season) p(winter area*year*season) | 5,801 | 1.05 | 0.31 | 85 | 1,479 |
| Φ(winter area*season) p(winter area*year*season) | 5,803 | 3.51 | 0.09 | 90 | 1,471 |
| Φ(constant) p(winter area*year*season) | 5,805 | 5.34 | 0.04 | 79 | 1,496 |
| Φ(season) p(winter area*year*season) | 5,806 | 5.84 | 0.03 | 80 | 1,495 |
Figure 2Fitness correlates for sanderlings wintering in different areas. Latitudes are those from the main study sites within winter areas. Dots are averages, and error bars indicate 95% confidence intervals. (a) Annual adult survival probabilities of six winter areas within Greenlandic sanderlings’ flyway. Survival estimates are those from the most parsimonious model from a set of 40 used to explain year‐round observation histories at and outside the study sites (See Materials and Methods and Table 2, Table S2). (b) Probability that juvenile relative to adult sanderlings migrated northwards in the summer following the winter during which individuals were caught and individually colour‐ringed in four winter areas. Estimates are based on a multi‐event mark–recapture model (see Materials and Methods). (c) Timing of northward migration through Iceland of sanderlings wintering in eight winter areas. The average timing of migration through Iceland is estimated from the most parsimonious linear mixed effects model with individual nested within year as random effects (see Materials and Methods). Day of year 140 represents 20 May. The 95% confidence intervals are based on a normal distribution for the survival probabilities and on a t‐distribution for the migration dates
Models for timing of northward migration through Iceland with different fixed effects. We fitted a random structure with individual nested within year (~1|Year/Individual) and varExp(form=~fitted(.)) as variance structure (Table S5) for all models. See Materials and Methods for explanation. The following parameters are shown: residual degrees of freedom (df), log‐likelihood (logLik), Akaike's information criterion (AIC), the difference in AIC with the top‐supported model (ΔAIC), model weights (w) and residual deviance (deviance)
| Model |
| logLik | AIC | ΔAIC |
| Deviance |
|---|---|---|---|---|---|---|
| Winter area | 18 | −5,420.84 | 10,877.7 | 0 | 0.67 | 10,841.7 |
| Winter area + Sex | 20 | −5,419.54 | 10,879.1 | 1.4 | 0.33 | 10,839.1 |
| Winter area * Sex | 34 | −5,412.31 | 10,892.62 | 15.0 | 0 | 10,824.6 |
| Sex | 13 | −5,535.13 | 11,096.3 | 218.6 | 0 | 11,070.3 |